Search results for "Pliocene"

showing 10 items of 28 documents

Plio-Pleistocene Dust Traps on Paleokarst Surfaces: A Case Study From the Carpathian Basin

2020

Plio-Pleistocene silt/clay-rich deposits and paleo-karst fissure sediments from sites of the northern and southern parts of the Carpathian Basin were investigated. These materials were supposed to be mixed during transport before being captured in karstified fissures. Evidence that the eolian fissure sediments of Plio-Pleistocene age in the older Triassic–Cretaceous limestones are derived from eolian silt and clay includes compositional and textural matches, especially decreasing grain-size trends observed downwards from the paleo-surface of the former landscape. Various environmental factors could be recognized by the statistical evaluation of grain-size distribution curves of fissure fill…

010504 meteorology & atmospheric sciencesPlioceneGeochemistryWeatheringclaySiltkarst010502 geochemistry & geophysics01 natural sciencesPaleosolPleistocenepaleosolLoessAeolian processesGeneral Earth and Planetary Scienceslcsh:QParent rockSiltstoneeolian sedimentationlcsh:ScienceSediment transportCarpathian basinGeology0105 earth and related environmental sciencesFrontiers in Earth Science
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Growth-increment characteristics and isotopic (delta O-18) temperature record of sub- thermocline Aequipecten opercularis (Mollusca: Bivalvia): evide…

2021

Abstract The shell δ18O of young modern Aequipecten opercularis from the southern North Sea provides an essentially faithful record of seasonal variation in seafloor temperature. In this well-mixed setting, A. opercularis shell δ18O also serves as a proxy for seasonal variation in surface temperature. Individuals from less agitated (e.g. deeper) settings in a warm climate would not be expected to record the full seasonal range in surface temperature because of thermal stratification in summer. Such circumstances have been invoked to explain cool isotopic summer temperatures from early Pliocene A. opercularis of eastern England. Support for a sub-thermocline setting derives from high-amplitu…

010506 paleontologybiologyδ18OPaleontologyOceanic climateSeasonality010502 geochemistry & geophysicsOceanographybiology.organism_classificationmedicine.disease01 natural sciencesAequipectenOceanographyMediterranean seaBivalve ; Hydrography ; Marine climate ; Pliocene ; SclerochronologySclerochronologymedicineThermoclineEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesEarth-Surface ProcessesTemperature record
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Effect of simulated faunal impoverishment and mixture on the ecological structure of modern mammal faunas: Implications for the reconstruction of Mio…

2011

15 pages; International audience; The strong link between environment and the ecological diversity of communities is often used for drawing palaeoenvironmental inferences from fossil assemblages. Here we focus on the reliability of fossil samples in comparison to original communities when inferring palaeoenvironments from the ecological diversity of fossil mammal faunas. Taphonomic processes and sampling techniques generally introduce two kinds of biases in fossil samples: 1) the directional impoverishment of communities, i.e. the absence of some specific categories of bones, individuals or species; and 2) the mixture of several communities, temporally (timeaveraging) and/or spatially (spac…

0106 biological sciences010506 paleontologyArboreal locomotionEcological diversityTaphonomyFaunaPalaeoenvironmentBiologyOceanography010603 evolutionary biology01 natural sciencesMio-PlioceneEcosystem diversityEcology Evolution Behavior and SystematicsMammal fauna[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontology0105 earth and related environmental sciencesEarth-Surface ProcessesEcologyPaleontologyInsectivore15. Life on landTaxonomic richnessAfricaPeriod (geology)MammalSpecies richness[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyPalaeogeography, Palaeoclimatology, Palaeoecology
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Distinct protoconchs recognised in three of the larger Mediterranean Cerithium species (Caenogastropoda: Cerithiidae)

2017

The gastropod genus Cerithium includes several polymorphic species which are hardly distinguishable using a morphological approach based on teleoconch characters. Here we show that protoconch characters can be reliably used to identify the larger Mediterranean species (Cerithium alucastrum, C. repandum and C. vulgatum), and to assess their intraspecific variability. Based on a large amount of morphological data, we show that a multispiral, strongly sculptured protoconch (traditionally associated with C. vulgatum) is found in C. alucastrum. This species originated in the Pliocene. A multispiral, weakly sculptured protoconch, not observed previously, is reported for C. vulgatum. A paucispiral…

0106 biological sciencesPlioceneCerithiumBiogeographyGastropodaZoology010502 geochemistry & geophysics010603 evolutionary biology01 natural scienceslarval developmenttaxonomyGastropodaAnthropoceneGeneticsEcology Evolution Behavior and Systematicsbiogeography0105 earth and related environmental sciencesCaenogastropodabiologyEcologyCerithiidaebiology.organism_classificationPleistoceneProtoconchAnimal Science and ZoologyTaxonomy (biology)Type localityecophenotype
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Petrography and carbonate isotope stratigraphy from MIS AND-1B core, Antarctica: Evidence of the early Pliocene warming event

2011

Abstract A large portion of ANDRILL (ANtarctic geological DRILLing) core AND-1B recovered in the Western Ross Sea and spanning the early Pliocene has been investigated in order to obtain a detailed carbonate isotope record from Antarctic margin sediments through the early Pliocene warming event. Petrographic observations and mineralogical analyses reveal the authigenic nature of the carbonate and small proportions of Fe and Mg incorporated within the calcite lattice. High productivity conditions testified by ~ 80 m-thick diatomite interval (383 to 460 mbsf) well fit with the composite nature of the authigenic carbonate generally characterizing organic matter-rich sediments. As is known, sed…

ANDRILLCalciteGlobal and Planetary Changegeographygeography.geographical_feature_categoryδ13CStable isotope ratioδ18OGlacierAuthigenicearly PlioceneOceanographypalaeoclimatePetrographychemistry.chemical_compoundPaleontologychemistrystable isotopeAntarcticaCarbonateGeologyGlobal and Planetary Change
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Witnesses of the early Pliocene sea-level rise in the Manilva Basin (Málaga, S Spain)

2020

The Sierra de la Utrera, a relief in the Manilva Basin (Malaga, SW Spain), shows bored surfaces at different heights above present-day sea level, from 96 m to 287 m. Borings occur in the eastern, central, and western parts of the Canuto de la Utrera, a prominent gorge in the central southern part of the relief excavated in Mesozoic limestones, as well as on the western end of the Canuto Chico, a smaller canyon in the northern part. Pliocene marine deposits fossilized the bored surfaces. Bored boulders of the substrate are embedded in the Pliocene sediments. The traces Gastrochaenolites ispp., Entobia ispp., Caulostrepsis ispp., Circolites kotoucensis, and Ericichnus asgaardi have been ident…

Canyongeography.geographical_feature_categoryEntobiaPaleontologyBiozoneArchaeologyGastrochaenolitesOnlapQE701-760PaleontologyGeographyIchnofaciesMesozoicbioerosion entobia ichnofacies palaeogeography early pliocene transgression sierra de utreraSea levelSpanish Journal of Palaeontology
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Paleoenvironmental evolution of the Pliocene Villarroya Lake, northern Spain. A multidisciplinary approach

2002

The Pliocene Villarroya basin fill consists of lacustrine and alluvial deposits over 100 m thick. The lacustrine deposits, up to 30 m thick, comprise three sequences. The two lower sequences consist of profundal, laminated deposits formed by mostly terrigenous facies that are overlain by charophytic carbonates and varves. The uppermost, third sequence made up of massive bioturbated mudstones corresponds to a very shallow lacustrine-palustrine environment. Bulk mineralogy comprises carbonates, clay minerals, quartz and feldspars. The carbonates are: exogenic, biogenic calcite and biogenic aragonite. Biogenic calcite constitutes ostracod shells and charophyte stem encrustations, whereas arago…

ClimateStratigraphyeducationplioceneengineering.materialPaleontologyOstracodProfundal zonemolluscsVarvebiologyTerrigenous sedimentAragonitelacustrine depositsGeologybiology.organism_classificationClay mineralogyCharophytesSource rockpollenostracodsIlliteengineeringSedimentary rockGeologySedimentary Geology
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Stratigraphic frame work of the type locality of Pirro Nord Mammal Faunal Unit (Late Villafranchian, Apricena south-eastern Italy)

2013

The fossiliferous karst deposits of the typical Pirro Nord Faunal Unit recently revived interest for the lithic tools documenting the human occurrence in southern Italy at Early Pleistocene. Therefore, a revision of the Pliocene to lowermost Pleistocene stratigraphic succession was needed. It was carried on with a twofold aim: to detail the stratigraphic architecture and the structural-depositional evolution of the “Apricena horst”, and to verify the chronostratigraphic constraints for the Pirro Nord F.U. in the type area of Apricena. The stratigraphic record has been subdivided in four units bounded by ubiquitous unconformity surfaces, often associated to evidence of sub-aerial exposure. F…

Facies Analysis Synsedimaentary faulting Pliocene Pleistocene Pirro Nord W GarganoSettore GEO/01 - Paleontologia E Paleoecologia
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The Monte San Nicola section (Sicily) revisited: A potential unit-stratotype of the Gelasian Stage

2022

The Monte San Nicola area (Southern Sicily) offers a spectacular exposure of open-marine sediments that were employed in 1998 for defining the Global Stratotype Section and Point (GSSP) of the Gelasian Stage (Upper Pliocene). After the lowering of the Pliocene/Pleistocene boundary to ca. 2.6 Ma in 2010, the Gelasian GSSP has been redefined as the base of both the Pleistocene Series and the Quaternary Period, which increased its importance and visibility within the scientific community. However, documentation on the Monte San Nicola reference section is still sparse. In the light of its renewed status, we decided to undertake a complete revision of the Gelasian Stage in its type area, in ord…

GSSPArcheologyGlobal and Planetary ChangeSettore GEO/02 - Geologia Stratigrafica E SedimentologicaStratigraphyPliocene-Pleistocene boundarymarine sedimentGeologySettore GEO/01 - Paleontologia E PaleoecologiaGelasianQuaternaryCalabrianmagnetostratigraphyEcology Evolution Behavior and Systematics
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THE GARGANO TERRE ROSSE INSULAR FAUNAS: AN OVERVIEW

2010

After forty years from its discovery, the history of the field surveys and of the researches on the fossiliferous deposits on Gargano is briefly reported. The Gargano fauna belongs to the Abruzzo-Apulian Palaeobioprovince (including also Scontrone and Palena, Abruzzo). The fossil assemblage comprehends all the classes of terrestrial vertebrates: Reptilia, Amphibia, Aves and Mammalia. The faunal composition is unbalanced and presents the features of a typical insular endemic fauna. The bulk of the assemblage is composed of small mammals and birds. Based on literature, we report the most characteristic features, phylogenetic relationships, and evolutionary remarks on a list of mammals, focusi…

Insular faunalcsh:GeologyLate Miocene-Early PlioceneGarganoBiogeographyLate Miocene-Early Pliocene; Gargano; Insular fauna; Endemism; Biochronology; Biogeographylcsh:Paleontologylcsh:QE1-996.5BiochronologySettore GEO/01 - Paleontologia E Paleoecologialcsh:QE701-760EndemismRivista Italiana di Paleontologia e Stratigrafia (Research In Paleontology and Stratigraphy)
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